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Milestones in the First 3 Billion Years of Life When Did the First Multicellular

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Milestones in the First 3 Billion Years of Life When Did the First Multicellular Milestones in the first 3 billion years of life • Origin of life - before 3.8 Ga • Origin of eukaryotes - before 1.4 Ga; before 2.7 Ga ? • Origin of multicellularity - 600-800 Ma ? • Origin of skeletons - 550 Ma ? • The Cambrian Explosion - 550-544 Ma ? When did the first multicellular eukaryotes arise? • Body fossils – “good” fossil evidence at 600-800 Ma – Questionable fossil evidence earlier (but stay tuned) • Molecular clocks – Wide variety of dates (600-1500 Ma) – Most dates focus on 800-1000 Ma 1 Grypania, ca. 2.1 Ga from Michigan Eukaryotic (triploblatic) Traces, India 1.0 or 0.6 Ga From Seilacher et al. 1998, Science 282: 80-83 2 Multicellular algae (?), Proterozoic (ca. 800 Ga), Montana and NW Canada 10 cm 3 (from Bromham & Hendy, Proc. R. Soc. Lond., 2000, 267:1041) Milestones in the first 3 billion years of life • Origin of life - before 3.8 Ga • Origin of eukaryotes - before 1.4 Ga; before 2.7 Ga ? • Origin of animals (multicellularity) - 600-800 Ma ? • Origin of skeletons - 550 Ma ? • The Cambrian Explosion - 550-544 Ma ? 4 Important points about the origin of skeletons • It really seems to have happened no earlier than ca. 550-600 Ma • Not just skeletonizing formerly soft-bodied critters; skeletons make new body plans possible. • Causes? Genetic innovation vs. environmental causes The oldest known skeletonized organism | 0.5 mm Cloudina – ca 550 Ma 5 Namacalathus, a calcified metazoan 550-543 Ma Namibia From Grotzinger et al., 2000 Paleobiology 26(3) Milestones in the first 3 billion years of life • Origin of life - before 3.8 Ga • Origin of eukaryotes - before 1.4 Ga; before 2.7 Ga ? • Origin of animals (multicellularity) - 600-800 Ma ? • Origin of skeletons - 550 Ma ? • The Cambrian Explosion - 550-544 Ma ? 6 The Cambrian Explosion The relatively sudden appearance and diversification of almost all of the phyla (all but Bryozoa) in the early Cambrian. This event began around 550 million years ago and lasted no more than 20-30 million years. The Linnean Hierarchy phylum class order family genus species 7 Major phyla of the fossil record • Porifera – sponges • Cnidaria – corals etc • Arthropoda – arthropods • Echinodermata – echinoderms • Brachiopoda – brachiopods • Bryozoa – bryozoans • Mollusca – mollusks • Chordata – vertebrates etc. Key Faunas Before/After the Cambrian Explosion: • Burgess Shale (505 Ma) • Chengjiang (520 Ma) • Small Shellies (Manykaian Stage) (544-530 Ma) • Ediacara (575-545 Ma) • Doushantuo embryos (580-570 Ma) 8 The Ediacara Biota The Ediacara Biota Parvancorina Dickensonia Cyclomedusa Tribrachidium Mawsonites 9 The Ediacara Biota Spriggina Charnia Ediacara fronds: Comparison with living Pennatulacean Cnidarians 10 The “traditional” interpretation of Ediacara (from Glaessner (1984) “Traditional” reconstructions of the Ediacara Biota 11 A radical alternative interpretation of the Ediacara Biota: Vendobionta (From Seilacher, 1989) Seilacher’s hypothesis • Ediacaran organisms (“vendobionts”) represent an independent origin of “animal-grade” multicellular eukaryotes • Vendobionts were immobile and possibly photosynthetic, photosymbiotic, chemosynthetic, or chemosymbiotic • They are not ancestral to any Phanerozoic forms • Ediacaran organisms all became extinct just before the Cambrian-Precambrian boundary 12 Spaniard's Bay in eastern Newfoundland. So is Seilacher correct? … probably not completely • Ediacaran forms now known from Cambrian • Taphonomy and new Ediacaran fossils show greater resemblances to Phanerozoic/modern forms possible • More detailed analysis of Ediacaran morphology suggests closer affinities to Phanerozoic/modern forms • But… there are still a lot of Problematica in Ediacara. 13 Why Seilacher’s hypothesis is important • Tests our assumptions • Implications for extraterrestrial life A Chordate in the Ediacara?? (2003) Length ca. 5 cm) 14 The latest on Ediacara… 2005 • There may be actual bilaterians among the Ediacaran biota • There are at least 3 biostratigraphically recognizeable assemblages: – Avalon 575-565 (e.g., Mistaken Point, Newfoundland) – Nama 565-550 – White Sea 550-545 The Ediacara Biota at Mistaken Point, Newfoundland http://geol.queensu.ca/museum/exhibits/ediac/mistaken_point/mistaken_pt.html 15 Key Faunas Before/After the Cambrian Explosion: • Burgess Shale (505 Ma) • Chengjiang (520 Ma) • Small Shellies (Manykaian Stage) (544-530 Ma) • Ediacara (575-545 Ma) • Doushantuo embryos (580-570 Ma) Doushantuo embryos http://more.abcnews.go.com/sections/science/DailyNews/fossils0204.html Bengtson & Zhao 1997, a SEM image depicting a suggested metazoan embryo – possibly Olivooides multisulcatus – at approximately the 256-cell stage. 16.
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